Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx

The Southern Ocean is responsible for approximately 40% of oceanic carbon uptake through biological and physical processes. In the Southern Ocean, phytoplankton growth is limited by low iron (Fe) and light supply. Climate model projections for the Southern Ocean indicate that temperature, underwater...

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Main Authors: Sarah M. Andrew, Hugh T. Morell, Robert F. Strzepek, Philip W. Boyd, Michael J. Ellwood
Format: Dataset
Language:unknown
Published: 2019
Subjects:
Online Access:https://doi.org/10.3389/fmars.2019.00681.s001
https://figshare.com/articles/Data_Sheet_1_Iron_Availability_Influences_the_Tolerance_of_Southern_Ocean_Phytoplankton_to_Warming_and_Elevated_Irradiance_xlsx/10127078
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record_format openpolar
spelling ftfrontimediafig:oai:figshare.com:article/10127078 2023-05-15T14:02:26+02:00 Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx Sarah M. Andrew Hugh T. Morell Robert F. Strzepek Philip W. Boyd Michael J. Ellwood 2019-11-01T15:12:57Z https://doi.org/10.3389/fmars.2019.00681.s001 https://figshare.com/articles/Data_Sheet_1_Iron_Availability_Influences_the_Tolerance_of_Southern_Ocean_Phytoplankton_to_Warming_and_Elevated_Irradiance_xlsx/10127078 unknown doi:10.3389/fmars.2019.00681.s001 https://figshare.com/articles/Data_Sheet_1_Iron_Availability_Influences_the_Tolerance_of_Southern_Ocean_Phytoplankton_to_Warming_and_Elevated_Irradiance_xlsx/10127078 CC BY 4.0 CC-BY Oceanography Marine Biology Marine Geoscience Biological Oceanography Chemical Oceanography Physical Oceanography Marine Engineering temperature climate change photosynthesis evolution multiple stressors carbon Dataset 2019 ftfrontimediafig https://doi.org/10.3389/fmars.2019.00681.s001 2019-11-06T23:50:14Z The Southern Ocean is responsible for approximately 40% of oceanic carbon uptake through biological and physical processes. In the Southern Ocean, phytoplankton growth is limited by low iron (Fe) and light supply. Climate model projections for the Southern Ocean indicate that temperature, underwater irradiance and Fe supply are likely to change simultaneously in the future due to increasing anthropogenic carbon dioxide emissions. The individual effects of these environmental properties on phytoplankton physiology have been extensively researched, and culturing studies using Southern Ocean phytoplankton have shown that temperature and Fe will play a key role on setting growth under future conditions. To explore the potential responses of Southern Ocean phytoplankton to these environmental changes, we cultured the haptophyte Phaeocystis antarctica and the diatoms Chaetoceros flexuosus, Proboscia inermis, and Thalassiosira antarctica under two light and iron combinations and over a range of temperatures. Our study revealed that the thermal response curves of key Southern Ocean phytoplankton are diverse, with the highest growth rates measured at 5°C (the annual temperature range at the isolation sites is currently 1–4°C). Warming had species-specific effects on the photochemical efficiency of photosystem II (PSII; F v /F m ), the functional absorption cross-section of PSII (σ PSII ), carbon:nitrogen ratio and cellular Chlorophyll a concentrations. Iron availability increased species’ ability to tolerate warmer conditions by increasing the upper limit for growth and subsequently increasing the thermal niche that each species inhabit. Dataset Antarc* Antarctica Southern Ocean Frontiers: Figshare Southern Ocean
institution Open Polar
collection Frontiers: Figshare
op_collection_id ftfrontimediafig
language unknown
topic Oceanography
Marine Biology
Marine Geoscience
Biological Oceanography
Chemical Oceanography
Physical Oceanography
Marine Engineering
temperature
climate change
photosynthesis
evolution
multiple stressors
carbon
spellingShingle Oceanography
Marine Biology
Marine Geoscience
Biological Oceanography
Chemical Oceanography
Physical Oceanography
Marine Engineering
temperature
climate change
photosynthesis
evolution
multiple stressors
carbon
Sarah M. Andrew
Hugh T. Morell
Robert F. Strzepek
Philip W. Boyd
Michael J. Ellwood
Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx
topic_facet Oceanography
Marine Biology
Marine Geoscience
Biological Oceanography
Chemical Oceanography
Physical Oceanography
Marine Engineering
temperature
climate change
photosynthesis
evolution
multiple stressors
carbon
description The Southern Ocean is responsible for approximately 40% of oceanic carbon uptake through biological and physical processes. In the Southern Ocean, phytoplankton growth is limited by low iron (Fe) and light supply. Climate model projections for the Southern Ocean indicate that temperature, underwater irradiance and Fe supply are likely to change simultaneously in the future due to increasing anthropogenic carbon dioxide emissions. The individual effects of these environmental properties on phytoplankton physiology have been extensively researched, and culturing studies using Southern Ocean phytoplankton have shown that temperature and Fe will play a key role on setting growth under future conditions. To explore the potential responses of Southern Ocean phytoplankton to these environmental changes, we cultured the haptophyte Phaeocystis antarctica and the diatoms Chaetoceros flexuosus, Proboscia inermis, and Thalassiosira antarctica under two light and iron combinations and over a range of temperatures. Our study revealed that the thermal response curves of key Southern Ocean phytoplankton are diverse, with the highest growth rates measured at 5°C (the annual temperature range at the isolation sites is currently 1–4°C). Warming had species-specific effects on the photochemical efficiency of photosystem II (PSII; F v /F m ), the functional absorption cross-section of PSII (σ PSII ), carbon:nitrogen ratio and cellular Chlorophyll a concentrations. Iron availability increased species’ ability to tolerate warmer conditions by increasing the upper limit for growth and subsequently increasing the thermal niche that each species inhabit.
format Dataset
author Sarah M. Andrew
Hugh T. Morell
Robert F. Strzepek
Philip W. Boyd
Michael J. Ellwood
author_facet Sarah M. Andrew
Hugh T. Morell
Robert F. Strzepek
Philip W. Boyd
Michael J. Ellwood
author_sort Sarah M. Andrew
title Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx
title_short Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx
title_full Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx
title_fullStr Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx
title_full_unstemmed Data_Sheet_1_Iron Availability Influences the Tolerance of Southern Ocean Phytoplankton to Warming and Elevated Irradiance.xlsx
title_sort data_sheet_1_iron availability influences the tolerance of southern ocean phytoplankton to warming and elevated irradiance.xlsx
publishDate 2019
url https://doi.org/10.3389/fmars.2019.00681.s001
https://figshare.com/articles/Data_Sheet_1_Iron_Availability_Influences_the_Tolerance_of_Southern_Ocean_Phytoplankton_to_Warming_and_Elevated_Irradiance_xlsx/10127078
geographic Southern Ocean
geographic_facet Southern Ocean
genre Antarc*
Antarctica
Southern Ocean
genre_facet Antarc*
Antarctica
Southern Ocean
op_relation doi:10.3389/fmars.2019.00681.s001
https://figshare.com/articles/Data_Sheet_1_Iron_Availability_Influences_the_Tolerance_of_Southern_Ocean_Phytoplankton_to_Warming_and_Elevated_Irradiance_xlsx/10127078
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.3389/fmars.2019.00681.s001
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